scholarly journals An Early Iron Age Camp of Reindeer Hunters in the Bolshezemelskaya Tundra, Nenets Autonomous Okrug

2019 ◽  
Vol 47 (3) ◽  
pp. 74-84
Author(s):  
A. M. Murygin ◽  
P. A. Kosintsev ◽  
T. I. Marchenko-Vagapova

This study outlines the fi ndings of excavations at More-Yu II—a site in the northern Bolshezemelskaya tundra. The habitation layer with numerous charcoal lenses was discovered inside the layer of buried soil overlain by eolian sand. Most fi nds are ceramics and animal bones. Arrowheads, o rnaments, tools, and ritual items are very rare. On the basis of palynological and faunal analyses, environmental changes from the sub-boreal warming until the end of the sub-Atlantic period are reconstructed. The temperature regime during the formation of cultural deposits was unstable. The principal subsistence strategy was reindeer hunting. The age of reindeer suggests that habitation periods coincided with cold seasons. Radiocarbon dates generated from reindeer bones point to the Early Iron Age. The camp dwellers were native reindeer hunters inhabiting the tundra belt of northeasternmost Europe. Ceramics representing the More-Yu type belong to the early stage of the Subarctic Pechora culture. They mark the Arctic component that became part of the n orthern Glya denovo population, abruptly changing the Finno-Permic culture of the taiga part of the Pechora basin in northern Urals.

2019 ◽  
Vol 8 (2) ◽  
pp. 171-179
Author(s):  
Alevtina Mikhailovna Kiseleva ◽  
Anton Igorevich Murashkin

Archaeological evidence for marine hunting and fishing at the coast of the Barents Sea dates from 5000 cal BC to 0 cal BC/AD, encompassing the Neolithic, the Early Metal Period and the Early Iron Age. Among hunting and fishing equipment are bone and antler harpoon heads, fishhooks and leisters. Four periods of development of the tools were established on the basis of stable occurrence of the artefacts types in complexes (semi-subterranean houses, shell middens, burials). The chronological boundaries of the periods were defined by the radiocarbon dates of this complexes: A - 5000-2500 cal BC, B - 2500-1600 cal BC, C - 1500-1100 cal BC, D - 900 cal BC - 0 cal BC/AD. The primary marine taxa exploited were pinnipeds and cetacean. The marine hunting was supplemented by catching Atlantic Cod and codfishes. Percentage ratio of animal bones from dated complexes indicates that the role of the seal and whale hunting had increased considerably since about 2500 cal BC. This coincides with the appearance of toggling harpoons in hunting equipment. The exploitation of aquatic resources in the Early Iron Age (after 900 cal BC) remained important in the subsistence economy. The transition to a primary exploitation of terrestrial resources at coastal locations is not observed.


AmS-Skrifter ◽  
2021 ◽  
pp. 1-300
Author(s):  
Trond Løken

The ambition of this monograph is to analyse a limited number of topics regarding house types and thus social and economic change from the extensive material that came out of the archaeological excavation that took place at Forsandmoen (“Forsand plain”), Forsand municipality, Rogaland, Norway during the decade 1980–1990, as well as the years 1992, 1995 and 2007. The excavation was organised as an interdisciplinaryresearch project within archaeology, botany (palynological analysis from bogs and soils, macrofossil analysis) and phosphate analysis, conducted by staff from the Museum of Archaeology in Stavanger (as it was called until 2009, now part of the University of Stavanger). A large phosphate survey project had demarcaded a 20 ha settlement area, among which 9 ha were excavated using mechanical topsoil stripping to expose thehabitation traces at the top of the glaciofluvial outwash plain of Forsandmoen. A total of 248 houses could be identified by archaeological excavations, distributed among 17 house types. In addition, 26 partly excavated houses could not be classified into a type. The extensive house material comprises three types of longhouses, of which there are as many as 30–40 in number, as well as four other longhouse types, of which there are only 2–7 in number. There were nine other house types, comprising partly small dwelling houses and partly storage houses, of which there were 3–10 in number. Lastly, there are 63 of the smallest storage house, consisting of only four postholes in a square shape. A collection of 264 radiocarbon dates demonstrated that the settlement was established in the last part of the 15th century BC and faded out during the 7th–8th century AD, encompassing the Nordic Bronze Age and Early Iron Age. As a number of houses comprising four of the house types were excavated with the same methods in the same area by the same staff, it is a major goal of this monograph to analyse thoroughly the different featuresof the houses (postholes, wall remains, entrances, ditches, hearths, house-structure, find-distribution) and how they were combined and changed into the different house types through time. House material from different Norwegian areas as well as Sweden, Denmark, Germany and the Netherlands is included in comparative analyses to reveal connections within the Nordic area. Special attention has been given to theinterpretation of the location of activity areas in the dwelling and byre sections in the houses, as well as the life expectancy of the two main longhouse types. Based on these analyses, I have presented a synthesis in 13 phases of the development of the settlement from Bronze Age Period II to the Merovingian Period. This analysis shows that, from a restricted settlement consisting of one or two small farms in the Early BronzeAge, it increases slightly throughout the Late Bronze Age to 2–3 solitary farms to a significantly larger settlement consisting of 3–4 larger farms in the Pre-Roman Iron Age. From the beginning of the early Roman Iron Age, the settlement seems to increase to 8–9 even larger farms, and through the late Roman Iron Age, the settlement increases to 12–13 such farms, of which 6–7 farms are located so close together that they would seem to be a nucleated or village settlement. In the beginning of the Migration Period, there were 16–17 farms, each consisting of a dwelling/byre longhouse and a workshop, agglomerated in an area of 300 x 200 m where the farms are arranged in four E–W oriented rows. In addition, two farms were situated 140 m NE of the main settlement. At the transition to the Merovingian Period, radiocarbon dates show that all but two of the farms were suddenly abandoned. At the end of that period, the Forsandmoen settlement was completely abandoned. The abandonment could have been caused by a combination of circumstances such as overexploitation in agriculture, colder climate, the Plague of Justinian or the collapse of the redistributive chiefdom system due to the breakdown of the Roman Empire. The abrupt abandonment also coincides with a huge volcanic eruption or cosmic event that clouded the sun around the whole globe in AD 536–537. It is argued that the climatic effect on the agriculture at this latitude could induce such a serious famine that the settlement, in combination with the other possible causes, was virtually laid waste during the ensuing cold decade AD 537–546. 


Author(s):  
YU. V. BOLTRIK ◽  
E. E. FIALKO

This chapter focuses on Trakhtemirov, one of the most important ancient settlements of the Early Iron Age in the Ukraine. During the ancient period, the trade routes and caravans met at Trakhtemirov which was situated over the three crossing points of the Dneiper. Its location on the steep heights assured residents of Trakhtemirov security of settlement. On three sides it was protected by the course of the Dnieper while on the other side it was defended by the plateau of the pre-Dneiper elevation. The ancient Trakhtemirov city is located around 100 km below Kiev, on a peninsula which is jutted into the river from the west. Trakhtemirov in the Early Iron Age was important as it was the site of the Cossack capital of Ukraine. It was also the site of the most prestigious artefacts of the Scythian period and a site for various items of jewellery, tools and weaponry. The abundance of artefacts in Trakhtemirov suggests that the city is a central place among the scattered sites of the middle course of the Dneiper.


Radiocarbon ◽  
2004 ◽  
Vol 46 (2) ◽  
pp. 933-941 ◽  
Author(s):  
Irina P Panyushkina ◽  
Steven W Leavitt ◽  
Alex Wiedenhoeft ◽  
Sarah Noggle ◽  
Brandon Curry ◽  
...  

The abrupt millennial-scale changes associated with the Younger Dryas (YD) event (“chronozone”) near the dawn of the Holocene are at least hemispheric, if not global, in extent. Evidence for the YD cold excursion is abundant in Europe but fairly meager in central North America. We are engaged in an investigation of high-resolution environmental changes in mid-North America over several millennia (about 10,000 to 14,000 BP) during the Late Glacial–Early Holocene transition, including the YD interval. Several sites containing logs or stumps have been identified and we are in the process of initial sampling or re-sampling them for this project. Here, we report on a site in central Illinois containing a deposit of logs initially thought to be of YD age preserved in alluvial sands. The assemblage of wood represents hardwood (angiosperm) trees, and the ring-width characteristics are favorable to developing formal tree-ring chronologies. However, 4 new radiocarbon dates indicate deposition of wood may have taken place over at least 8000 14C yr (6000–14,000 BP). This complicates the effort to develop a single floating chronology of several hundred years at this site, but it may provide wood from a restricted region over a long period of time from which to develop a sequence of floating chronologies, the timing of deposition and preservation of which could be related to paleoclimatic events and conditions.


Author(s):  
Daniel Pioske

Chapter 2 begins a series of case studies that are devoted to exploring what knowledge was drawn on by the biblical scribes to develop stories about the early Iron Age period. This chapter’s investigation is devoted to the Philistine city of Gath, one of the largest cities of its time and a site that was destroyed ca. 830 BCE. Significant about Gath, consequently, is that it flourished as an inhabited location before the emergence of a mature Hebrew prose writing tradition, meaning that the information recounted about the city was predicated primarily on older cultural memories of the location. Comparing the biblical references to the site with Gath’s archaeological remains reveals moments of resonance between these stories and the material culture unearthed from the location. Accordingly, what comes to light through this chapter’s analysis is one mode of remembering that informed the creation of these biblical stories: that of resilience.


Radiocarbon ◽  
2004 ◽  
Vol 46 (1) ◽  
pp. 353-362 ◽  
Author(s):  
Yaroslav V Kuzmin ◽  
Alexander A Vasilevski ◽  
Sergei V Gorbunov ◽  
G S Burr ◽  
A J Timothy Jull ◽  
...  

A chronological framework for the prehistoric cultural complexes of Sakhalin Island is presented based on 160 radiocarbon dates from 74 sites. The earliest 14C-dated site, Ogonki 5, corresponds to the Upper Paleolithic, about 19,500–17,800 BP. According to the 14C data, since about 8800 BP, there is a continuous sequence of Neolithic, Early Iron Age, and Medieval complexes. The Neolithic existed during approximately 8800–2800 BP. Transitional Neolithic-Early Iron Age complexes are dated to about 2800–2300 BP. The Early Iron Age may be dated to about 2500–1300 BP. The Middle Ages period is dated to approximately 1300–300 BP (VII–XVII centuries AD).


1924 ◽  
Vol 4 (2) ◽  
pp. 211-233
Author(s):  
Cyril Fox

It is remarkable that so few attempts have been made to illustrate continuity of settlement on a given site through successive culture phases in East Anglia. No more valuable study could be undertaken by any field archæologist, than the careful examination of successive deposits on such a site. Especially useful would be the analysis of the transitional phases, showing the extent to which the art and craft-workers of one period influenced the technique and style of their successors and descendants; such a study should also throw light on the material, social and economic effects on the peasantry of the district of invasion and conquest, an evil from which East Anglia seems to have suffered every 500 years or so from about 1000 B.C. onwards. I cannot offer you, first hand, such a study; but it may be worth while, as an approach to the ideal, to illustrate a collection of objects from a settlement which seems to have been occupied during three (or four) culture phases for a total period of some 2,000 years.


Radiocarbon ◽  
2021 ◽  
pp. 1-22
Author(s):  
Steinar Solheim

ABSTRACT The paper explores the emergence and development of arable farming in southeastern Norway by compiling and analyzing directly dated cereals from archaeological contexts. By using summed probability distributions of radiocarbon dates and Bayesian modeling, the paper presents the first comprehensive analysis of the directly dated evidence for farming in the region. The models provide a more precise temporal resolution to the development than hitherto presented. The results demonstrate that the introduction of arable farming to southeastern Norway was a long-term development including several steps. Three different stages are pointed out as important in the process of establishing arable farming: the Early and Middle Neolithic, the Late Neolithic, and the Early Iron Age.


Author(s):  
Xin Wang ◽  
Xue Shang ◽  
Colin Smith ◽  
Dong Wei ◽  
Jie Zhang ◽  
...  
Keyword(s):  
Iron Age ◽  

2020 ◽  
Author(s):  
Giorgi Kirkitadze ◽  
Mikheil Elashvili ◽  
Levan Navrozashvili ◽  
Mikheil Lobjanidze ◽  
Levan Losaberidze ◽  
...  

<p>Studying of the interactions between past environmental changes and former human societies delivers key information to understand the future evolution of landscapes under changing environmental conditions and increasing human stress. The combination of these two factors is especially critical for fragile landscapes such as drylands, where even small-scale climatic or anthropogenic factors can have relatively large effects on the landscape dynamics.</p><p>Holocene paleoenvironmental changes on the Shiraki Plain, located in Eastern Georgia (South Caucasus), were studied. The selected site is characterized by semiarid climate conditions (annual precipitation <500 mm per year) and an open dry steppic landscape today. Currently the area is devoid of settlements, due to absence of water resources. However, recent archaeological data collected using remote sensing and ground-proven by ongoing archaeological excavations, delivered evidences of an active former human inhabitation of this area mostly during the Late Bronze - Early Iron Ages. Several large, city-type settlements of the given period that were identified on the Shiraki Plain suggest the existence of early state formation under favorable environmental conditions.</p><p>During the conducted study we have combined stratigraphical-sedimentological investigations of sediments using drilling cores, trenches and laboratory analyses with high-resolution D-GPS measurements in the RTK mode, remote sensing using drone photogrammetric surveys, paleoecological investigations, and hydrological modeling. Our initial results clearly support the hypothesis of a large shallow lake in the center of the Shiraki Plain that was surrounded by the Late Bronze and Early Iron Age settlements. Therefore, the regional water balance of that period was obviously more positive than today. Furthermore, our investigations indicate that this period of high settlement intensity was characterized by intensive soil erosion processes that washed away the dominant Chernozem soils.</p><p>Altogether, our investigations suggest a tipping point of the landscape evolution dynamics that must have been crossed during the Late Bronze and Early Iron period, leading to the current dry steppic landscape. This also provides key information to reconstruct the archaeological past of the region, and to address the main question of rapid depopulation and further abandonment of this area.</p>


Sign in / Sign up

Export Citation Format

Share Document